Quick Links
Title     |     Introduction     |     Electromagnetic Radiation     |     Photons Traveling to Earth     |     Photoelectric Effect     |     Sources






Electromagnetic Radiation

Electromagnetic radiation harnessed for energy on Earth originates at the Sun. In one second the Sun generates as much energy as 1 trillion megaton bombs. The Sun is very massive at about kg and it is composed of about 75% hydrogen and most of the rest is helium. The massive size of the Sun creates an enormous gravitational force that pulls the Sun's surroundings inward. The large inward pressure is responsible for the nuclear fusion reactions in hydrogen atoms. Electromagnetic radiation can be explained through the process and repercussions of the nuclear fusion of hydrogen atoms.

X 1 Trillion = Sun's Energy Production Every Second!
                                                cog-ff.com


The Sun is composed of three main regions: the core, the radiative zone and the convective zone. The core is where the enormous amounts of energy are created which give creation to photons. Photons are the particles/waves that make up light; photons oscillating at different frequencies become different light, waves, and rays. Photons exit the core into the radiative zone, then to the convective zone, out of the Sun's atmosphere, and finally into space.


en.wikipedia.org
The Core
The energy that is made in the core is released and carried outward by photon-light units. The initial reaction to produce energy comes from two single proton hydrogen ions and a great amount of pressure. The hydrogen ions fuse and start to produce other atoms, ions, particles, and energy where mass is lost in the creation.

Physics of Nuclear Fusion Between Hydrogen Atoms in the Sun's Core

Nuclear fusion is the process of atom's nuclei joining. Hydrogen When two hydrogen atoms undergo nuclear fusion they release energy in the process. When the two hydrogen atoms fuse they create different atoms and ions which also interact with more of the atoms and ions. The reactions that take place between the atoms and ions produce energy eventually in the form of photons with frequencies ranging across the electromagnetic spectrum. The following table accounts for 85% of the energy produced in the core of the Sun:




The underlying physics seen in the processes in the above table can be related with Einsteins theory of relativity. When a less massive product comes out of the reaction between atoms and ions, the mass difference can be accounted for through energy conversion using the equation below where E is the energy, m is the mass, and c is the (constant) speed of light.



The processes above account for approximately 85% of the produced energy in the Sun. The other 15% comes from interactions between helium-3, helium-4, beryllium-7, lithium-7, protons, electrons, and neutrinos. When the initial nuclear fusion between hydrogen isotopes takes place it paves the way for the resulting reactions, atoms, and ions. The different interactions with atoms and ions allow for photons to be released with different frequencies. The frequencies of the photons produced range across the electromagnetic spectrum and simply put all of the different frequencies account for the different types of light, waves, and rays produced by the Sun.



The Radiative Zone and Convective Zone
Photons carry the energy from the core outward and is thus a photon made by the core. Photons are absorbed in the radiative zone by gas molecules after traveling only 1 micron. A gas molecule absorbs a proton, gets heated up by the absorption, and re-emits an identical photon which will have the same wavelength and frequency. The cycle of gas molecules absorbing protons continues and a single photon goes through approximately of these absorptions before finally reaching the surface of the radiative zone and being re-emitted into the convective zone. Once in the convective zone photons continue to be carried outward. In the convective zone photons are carried outward to the Sun's surface by convective currents at a faster rate than in the core or radiative zone.